Vector acoustic measurements of underwater noise made continually over a 24-h period within a small bay on the west side of Puget Sound, Washington State are discussed. The bay contains the Washington State ferry landing at Kingston with measurement site approximately 1 km distant from the landing, at water depth 42 m. Periodic, nearby ferry traffic, and episodic large-vessel shipping activity punctuate the observations which will be compared with those made in deeper waters. Potential and kinetic energies in key shipping decidecimal bands are equal within calibration uncertainty; a practical result towards the inference of kinematic properties from pressure-only measurements within inland waters complementing similar results obtained in off shore waters. An important exception exists when the noise field is dominated by a vessel passing directly over the sensor, as was demonstrated by the deployment vessel moving at speed 7.5 knots. Observed near the seafloor, broadband noise emissions from a vessel passing directly above exhibit frequency bands where potential acoustic energy is greater than kinetic energy (and vice versa in neighboring frequency bands). This phenomenon is also examined with a model based on multiple interfering reflections from the seabed, sea surface, and buried sediment layers.
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